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Lanai Volcano

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Lanai Volcano

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along with plantation course at kapalua together with las vegas villas together with make a point to visit this mauis iao needle also atlantis submarine tours as well as island sightseeing tours along with hawaii vacation news deals january 23 2013 as well as the state of hawaii in addition best places big island hawaii also police investigate threat at kaiser high school moreover lava entering water hawaii island together with ancient hawaiian carved wood statue nice position moreover why world keeps falling love waikiki in addition kauai beach splash along with old pali road haunted hawaii further park shore waikiki as well as fact 3 of 50 about hawaii the hawaiian alphabet further file high clouds seen from maui also hawaii weather along with update closed iao valley maui travelers. Atlantis Submarine Tours also Island Sightseeing Tours moreover Fact 3 Of 50 About Hawaii The Hawaiian Alphabet also Park Shore Waikiki additionally Hawaii Vacation News Deals January 23 2013.
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LANAI. Hawaii. Type: Shield volcano Lat/Long: 20.83°N, 158.92°W Shield Dimensions: Length: 60 km Maximum width: 50 km Elevation: 1.030 m: 5.5km above ocean floor Caldera Dimensions: Palawai Basin: 5 km wide x >250 m deep Miki Basin: 2 km wide x >30 m deep Eruptive History: Growth of northeast flank 1.81.4 Ma Growth of southwest Jlank 1.41.2 Ma Composition: Tholeiitic basalt Major vopt b««ak i W •"••" • '.. '? ". •~\ SX / 3 :''' N ftiCa' W  Comparison of the degree of weathering and erosion of the older Hawaiian volcanoes, such as the Waianae and Koolau volcanoes on Oahu, and the Kauai and Niihau volcanoes, to that of similar rocks of known geologic ages in other parts of the

world.suggests that these volcanoes must have ceased activity well over a million years ago. Using the rate of burial of the trunks of kiawe trees on the island of Lanai by debris eroded from the higher parts of the island since the introduction HISTORY. From. Volcanoes. to. the. Present. The wisdomfrom thepast will help us with thefuture. —Charles Ka'upu Hawai'i's volcanic origins and isolation in the Pacific have led to extraordinary beauty, unusual flora and fauna, and unique history, which is recent in geologic time and human habitation. Volcano (submarine) near Island 30 km (to southeast) 0 of Hawaii Kilauea Volcano on Island of Hawaii 0 km 00.4 Mauna Kea Volcano on Island 54 km (to northwest) 0.4 of Hawaii

Haleakala.Volcano on east Maui Island 182 km (to northwest) 0.8 Kahoolawe Volcano and Island 185 km (to northwest) 1.0 (southwest of Maui Island) Kahalawai Volcano on west Maui 221 km (to northwest) 1.3 Island Lanai Volcano on Lanai Island 226 km (to northwest) 1.3 East Molokai Volcano on 256 The tholeiitic shield stage is known to form the major portion of the subaerial and, we assume, the submarine part of each volcano. On the main islands, only Hualaiai Volcano and Kaula Island do not have subaerial exposures of tholeiitic lavas. Alkalic postshield stage lava occurs late in the eruptive sequence and has not yet developed on Loihi. Kilauea. or Mauna Loa volcanoes. To the west it occurs on all volcanoes except Lanai and Koolau.

although.the volumes present on Kauai.KAHOOLAWE AND LANAI Each of these islands consists of a single shield volcano with a summit caldera, and each has been little dissected. KAHOOLAWE VOLCANO The lava of Kahoolawe Volcano was erupted along a prominent southwest rift zone (fig. 1.25). The caldera was almost completely buried beneath a cap of later lava. The rocks that form essentially all of the Island of Kahoolawe, the smallest of the major islands, were called the Kanapou Volcanic Series by Stearns Despite the shieldlike shape of Hawaiian volcanoes, with their gently sloping flanks, many of the islands are bordered by steep scarps, some of them hundreds of meters high. Some form spectacular cliffs on the islands themselves (most

notably.on Kauai and Molokai), and some are hidden beneath the sea around individual islands (Hawaii) or groups of islands (Oahu, Molokai, Lanai, and Maui). Known as pali in Hawaiian, these scarps represent eroded faults along which large slices Among the Hawaiian Islands proper, rocks were collected from Maui, Molokai and Lanai. In Molokai, there are nearly eighty alkalic basaltic flows that make up the Kalaupapa section on the northern side of the island. A dozen samples were selected for this study that come from the horizons for which Beeson (1976) provided petrographic and petrochemical data. Additional samples were collected from the posterosional Kalaupapa volcano near the old leper colony at Kalawao and Lanai Volcanic

Series.Lanai Basalt1 Pliocene and Pleistocene ( ?) : Lanai Island, Hawaii. Original reference : C. K. Wentworth, 1925, Bernice P. Bishop Mus. Bull. 24, p. 34. H. T. Stearns, 1946, Hawaii Div. Hydrography Bull. 9, p. 67; G. A. Mac donald and D. A. Davis in Jacques Avias and others, 1956, Lexique Strat. Internat., v. 6, Oceanie, fasc. 2, p. 110. Thinl>edded and pahoehoe basaltic flows, a few mixed cinder and spatter cones ; about 375 feeding dikes. Composes cone of Moore reports that Gloria also found many drowned coral reefs descending in steplike order to depths of almost 2 kilometres off Maui, Lanai and the island of Hawaii. The reefs formed over the past 650 000 years, with the oldest one at the bottom. Dating of the reefs, says

Moore,.has confirmed that the southeastern section 2: Eruptions keep to a timetable Volcano shape at peak. coming months — that Loihi may be a dying volcano. For the moment at least, scientists still regard Loihi as 

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